Abstract
The new biostratigraphyc data and the revision of the old data, suggest us to show for this one age Upper Cenomanien up to Middle Turonian. The distribution of the different sediments and the relations among the different Litostrati, graphic units, we can explain by the development of a Cycle. This Cycle is formed by one fast transgression of the open Shelf, followed by a progradation of the near Shelf. All of this evolution is in relation with too eustatic changos of the sea level.
Highlights
Summary
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.